It's a residual mountain(unaka) which were a set of thrust blocks under the erosion unconformity.It's reservoir pore space is a fracture-vug-pore system of Ordovician carbonate karst.
该气藏构造为道冲构造侵
而成
山,储集体为
陶系碳酸盐
缝洞孔体系,流体呈层状分布(集中分布于
陶系峰峰组和上马家沟组上段)。